留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

西南天山乌什县晚三叠世镁铁-超镁铁质层状杂岩体年代学及地球化学研究

胡朝斌 李培庆 辜平阳 陈锐明 查显锋 庄玉军

胡朝斌, 李培庆, 辜平阳, 等, 2016. 西南天山乌什县晚三叠世镁铁-超镁铁质层状杂岩体年代学及地球化学研究. 地质力学学报, 22 (4): 1015-1031.
引用本文: 胡朝斌, 李培庆, 辜平阳, 等, 2016. 西南天山乌什县晚三叠世镁铁-超镁铁质层状杂岩体年代学及地球化学研究. 地质力学学报, 22 (4): 1015-1031.
HU Chao-bin, LI Pei-qing, GU Ping-yang, et al., 2016. GEOCHRONOOGICAL AND GEOCHEMICAL STUDY OF THE LATE TRIASSIC LAYERED MAFIC-ULTRAMFIC INTRUSIONS IN BEISHAN AREA OF WUSHI COUNTY, SOUTHWEST TIANSHAN. Journal of Geomechanics, 22 (4): 1015-1031.
Citation: HU Chao-bin, LI Pei-qing, GU Ping-yang, et al., 2016. GEOCHRONOOGICAL AND GEOCHEMICAL STUDY OF THE LATE TRIASSIC LAYERED MAFIC-ULTRAMFIC INTRUSIONS IN BEISHAN AREA OF WUSHI COUNTY, SOUTHWEST TIANSHAN. Journal of Geomechanics, 22 (4): 1015-1031.

西南天山乌什县晚三叠世镁铁-超镁铁质层状杂岩体年代学及地球化学研究

基金项目: 

中国地质调查局地质调查项目“特殊地质地貌区填图试点” DD20160060

“新疆1:5万喀伊车山口等3幅艰险区试点项目” 12120114042701

“东昆仑成矿带木孜塔格铅锌铜金多金属矿调查评价区地质矿产调查” DD20160002

详细信息
    作者简介:

    胡朝斌(1990-), 男, 助理工程师, 岩石地球化学专业。E-mail:405825740@qq.com

  • 中图分类号: P595;P597

GEOCHRONOOGICAL AND GEOCHEMICAL STUDY OF THE LATE TRIASSIC LAYERED MAFIC-ULTRAMFIC INTRUSIONS IN BEISHAN AREA OF WUSHI COUNTY, SOUTHWEST TIANSHAN

  • 摘要: 镁铁-超镁铁质层状杂岩体被认为是岩石圈伸展的重要标志之一,携带有丰富的地幔信息,是研究地幔物质组成、深部地质作用的绝佳对象。西南天山乌什县北巴勒的尔喀克沟地区新发现的镁铁-超镁铁质岩体具有层状杂岩特征,获得辉长岩锆石U-Pb年龄为224±4 Ma,属于晚三叠世。岩石地球化学分析显示富水、富碱、轻稀土富集、重稀土亏损以及明显富集Th、U、Nb、Ta、La、Ce不相容元素等特征,指示其源自于含水的富集型地幔源区,是石榴石二辉橄榄岩较低程度部分熔融的产物。其原生岩浆可能为富铁、钛的高镁玄武质岩浆,岩石系列主要受分离结晶作用控制,同化混染作用影响小。该期岩浆活动于南天山洋盆闭合、板块的碰撞造山活动之后的陆内造山阶段,代表了板块拉伸背景下幔源岩浆演化的产物,指示西南天山地区在三叠纪末可能存在一期岩石圈伸展事件。

     

  • 图  1  研究区区域地质示意图(a, 底图修改自杨树锋等[28])及研究区地质简图(b)

    Figure  1.  Regional geological map and geological sketch map of study area

    图  2  巴勒的尔喀克沟岩体野外宏观特征

    Figure  2.  Outcrop photos of the layered Mafic-ultramafic intrusions

    图  3  巴勒的尔喀克沟岩体岩石镜下特征

    a—橄辉岩(-); b—蛇纹石化、透闪石化橄辉岩(+); c—含橄榄辉石岩(+); d—辉长岩(+); e—辉石闪长岩(+); f—闪长岩(-); Ol—橄榄石; Opx—斜方辉石; Cpx—单斜辉石; Tr—透闪石; Ser—蛇纹石; Hb—角闪石; Pl—斜长石; Mt—磁铁矿; Ilm—钛铁矿; Ap—磷灰石

    Figure  3.  Microscope characteristics of the Baladikagou pluton

    图  4  辉长岩锆石阴极发光图像、U-Pb年龄协和图

    Figure  4.  CL images of zircons, U-Pb concordia diagram

    图  5  Zr/TiO2*0.0001-Nb/Y图解[32]

    Figure  5.  Zr/TiO2*0.0001-Nb/Y diagram

    图  6  稀土元素球粒陨石标准化配分模式图(左)、微量元素原始地幔标准化蛛网图(右)

    Figure  6.  Chondrite-normalized REE patterns (left) and Spider plot of trace element of samples (right)

    图  7  Zr-Nb和Zr-Y图解[40](图例同图 6)

    Figure  7.  Diagrams of Zr-Nb and Zr-Y

    图  8  球粒陨石标准化(Tb/Yb)N-(La/Sm)N[41]和Ce/Y-Zr/Nb[42]图解(图例同图 6)

    Figure  8.  The chondrite-normalized (Tb/Yb)N-(La/Sm)N and Ce/Y-Zr/Nb diagrams

    图  9  Th/Nb-SiO2、Nb/La-SiO2、K2O/TiO2-SiO2、La/Sm-La图解(图例同图 6)

    Figure  9.  Diagrams of Th/Nb-SiO2, Nb/La-SiO2, K2O/TiO2-SiO2 and La/Sm-La

    图  10  哈克图解(图例同图 6)

    Figure  10.  Harker variation diagram

    表  1  辉长岩(5004-3) 锆石U-Pb同位素分析结果

    Table  1.   Zircon U-Pb Isotopic analysis composition of gabbro (5004-3)

    分析号Pb/10-6Th/10-6U/10-6Th/U年龄/Ma比值协和度
    207Pb/206Pb1σ207Pb/235U1σ206Pb/238U1σ207Pb/206Pb1σ207Pb/235U1σ206Pb/238U1σ
    5004/3/11051725950.29487.2122.49244.312.18219.73.690.05690.0030.27200.0150.034670.00060.11
    5004/3/2361161980.59328.9157.34237.115.14227.84.340.05300.0040.26310.0190.035970.00070.04
    5004/3/329911610.56325.5227.15234.322.01225.15.640.05290.0060.25960.0270.035540.00090.04
    5004/3/4801944430.44221.7155.43229.814.21230.44.300.05060.0040.25400.0180.036390.00070
    5004/3/517732810570.31575.780.48249.88.24216.32.980.05920.0020.27890.0100.034120.00050.15
    5004/3/6512302700.85269.6173.93221.815.63217.14.460.05160.0040.24420.0190.034250.00070.02
    5004/3/7472352510.94174.0188.49214.516.22218.04.620.04960.0040.23530.0200.034390.0007-0.02
    5004/3/81122656320.42467.5120.60251.112.21228.13.810.05640.0030.28050.0150.036020.00060.1
    5004/3/91506638110.82220.1142.26229.012.90229.64.050.05050.0030.25300.0160.036250.00070
    5004/3/101086135461.12339.5114.16237.710.86227.23.590.05330.0030.26380.0140.035870.00060.05
    5004/3/1153254332930.16468.577.53245.77.68222.93.150.05640.0020.27380.0100.035180.00050.1
    5004/3/12631173540.33253.6323.41221.330.24218.27.910.05130.0080.24350.0370.034430.00130.01
    5004/3/13796193791.63253.6368.79233.536.71231.66.550.05130.0090.25850.0460.036580.00150.01
    5004/3/14502092640.79435.0178.48246.318.10227.25.100.05560.0050.27460.0230.035880.00080.08
    5004/3/151123066530.47382.1115.05239.111.14225.13.770.05430.0030.26550.0140.035530.00060.06
    5004/3/16842174650.47595.1137.03263.614.93228.14.410.05980.0040.29640.0190.036020.00070.16
    5004/3/17702753970.69238.6165.99224.314.95223.34.530.05100.0040.24720.0180.035250.00070
    下载: 导出CSV

    表  2  样品全岩主量(%)及微量元素(10-6)分析结果

    Table  2.   Major elements and trace elements analysis data

    样品编号5009-95009-105009-185009-195009-205016-25016-45016-75002-55016-45011-25011-35042-3HF-39-35004-35015-45013-1
    岩性橄辉岩橄辉岩橄辉岩橄辉岩橄辉岩橄辉岩橄辉岩辉石岩辉石岩辉石岩辉石岩辉石岩辉石岩辉长岩辉长岩辉长岩辉长岩
    SiO242.5542.6344.8344.5244.1844.3843.7344.6242.3243.7341.2040.5042.1646.3448.0242.8639.89
    AI2O36.957.086.426.536.677.9610.426.8011.3610.429.649.8210.3611.4312.6410.6110.82
    Fe2O34.053.402.782.732.462.451.802.822.461.801.821.891.842.032.151.691.71
    FeO8.258.608.108.358.659.3510.208.8210.9010.209.6510.7010.359.108.059.8010.00
    CaO8.9210.2010.6110.9011.3710.449.1111.756.629.1110.529.827.076.526.586.747.92
    MgO19.6519.0818.8118.4118.0716.0812.6316.8612.5912.6313.5314.1214.889.298.3610.3310.35
    K2O0.090.100.140.160.150.701.130.500.841.130.880.740.591.382.990.100.26
    Na2O0.220.220.340.330.300.901.670.442.081.671.431.230.231.472.761.101.17
    TiO21.941.791.831.951.952.392.762.222.972.762.632.763.383.003.022.752.80
    P2O50.230.250.260.260.280.350.430.290.450.430.280.400.540.490.530.420.46
    MnO0.130.140.160.170.190.170.190.180.190.190.190.210.220.150.140.170.19
    灼失※6.526.045.235.215.304.445.594.287.005.597.867.438.038.524.4613.1214.12
    H2O+5.123.963.043.763.522.162.862.344.122.862.562.824.602.962.464.563.00
    FeOt11.8911.6610.6010.8110.8611.5511.8211.3613.1111.8211.2912.4012.0110.939.9811.3211.54
    Fe2O3t13.2212.9611.7812.0112.0712.8413.1412.6214.5713.1412.5413.7813.3412.1411.1012.5812.82
    Mg#77.6077.4478.8278.1377.7274.4869.1475.6966.8169.1471.5470.4872.2264.0763.7165.6865.29
    La22.5026.2028.0026.7025.9033.2027.634.34846.442.242.863.147.0051.3046.5048.50
    Ce50.4055.4056.4055.8056.0068.3058.472.697.294.18787.213196.70105.0091.8095.90
    Pr6.626.7807.087.117.248.747.529.2211.811.410.610.615.911.6012.9011.0011.40
    Nd27.2026.8027.6029.0028.5036.2030.0035.946.544.442.142.163.147.6052.2041.9042.10
    Sm5.925.405.725.956.027.406.587.688.748.938.388.1211.29.559.928.108.55
    Eu1.871.771.751.831.822.201.892.122.722.772.512.283.322.653.062.152.30
    Gd5.084.685.004.955.026.325.786.797.587.437.056.938.838.318.006.777.12
    Tb0.790.710.770.780.760.960.800.951.171.1110.951.341.141.230.950.95
    Dy3.713.393.533.613.724.454.164.855.385.265.054.926.035.665.834.794.97
    Ho0.640.620.630.620.670.820.700.920.940.950.920.881.041.041.020.850.84
    Er1.601.551.571.551.671.981.702.322.42.312.252.222.662.642.582.122.16
    Tm0.220.210.210.220.240.260.240.330.320.310.30.30.350.370.350.290.3
    Yb1.291.251.251.311.401.561.372.051.931.851.891.772.182.272.141.701.84
    Lu0.190.180.180.200.210.220.200.310.280.260.260.240.30.340.320.240.26
    Y15.5014.615.2015.2015.9018.8017.0021.622.521.721.620.824.725.0025.3020.3021.50
    ∑REE143.53149.54154.89154.83155.07191.41163.94201.94257.46249.18233.11232.11335.05261.87281.15239.46248.69
    LREE114.51122.35126.55126.39125.48156.04131.99161.82214.96208.00192.79193.10287.62215.10234.38201.45208.75
    HREE29.0227.1928.3428.4429.5935.3731.9540.1242.5041.1840.3239.0147.4346.7746.7738.0139.94
    LREE/HREE3.954.504.474.444.244.414.134.035.065.054.784.956.064.605.015.305.23
    δEu1.021.050.981.000.980.960.920.881.001.010.970.910.990.891.020.860.88
    LaN/YbN12.5115.0316.0714.6213.2715.2714.4512.0017.8417.9916.0217.3420.7614.8517.2019.6218.91
    LaN/SmN2.453.133.162.902.782.902.712.883.553.353.253.403.643.183.343.713.66
    GdN/YbN3.263.103.313.132.973.353.492.743.253.323.093.243.353.033.093.293.20
    Cu123105.00222.00265.00127.0095.80141.0078.812415198.6015415092.50276.0089.288.2
    Pb2.712.593.523.833.022.892.707.723.8412.63.276.84.689.632.775.646.21
    Zn97.4089.3096.5098.30110.00118108.00139136120116129183170.0090.80121.00124.00
    Cr1740.001860.001740.001660.001620.0013401520.00980.00691.00744.00915.001060.00652452.00202.00578.00521.00
    Ni703.00790.00759.00725.00704.00485542.00456397326.00392.00458313.00159.00115.00262.00248.00
    Co83.6083.0090.6087.6081.3068.773.6072.568.157.8060.6066.360.5046.4042.1055.6053.60
    Li25.4019.5021.1021.9014.3044.938.8051.330.246.4055.7060.946.5046.8020.10102.00100.00
    Rb5.344.005.486.136.5949.341.0032.238.547.4019.7020.843.9090.2058.606.036.50
    Cs1.501.471.282.131.3713.69.247.088.662.192.503.547.7017.404.160.860.45
    Sr87.4088.2094.8091.2088.8011296.8163255323792499.00173.00402.00402.00439.00523.00
    Ba44.6047.4061.1054.8045.0081.791.2145302724779.00510.0086.40290.001360.0092.80139.00
    V236.00224.00205.00214.00216.00256250293261301273.00304313.00310.00301.00284.00293.00
    Sc29.0032.7036.4040.4040.8035.437.42820.930.629.1029.928.9027.0022.0025.8026.70
    Nb22.9023.0024.4023.5024.3029.524.936.945.843.642.7038.556.2050.4049.8043.5046.30
    Ta2.022.042.042.022.052.261.952.823.463.12.902.74.063.783.353.023.12
    Zr146.00145.00158.00160.00167.00201170218275246250.00236349272290261270
    Hf4.494.244.714.694.855.644.975.947.227.097.006.639.607.347.896.907.18
    Be0.370.700.870.930.881.111.021.591.611.522.081.821.561.541.331.191.30
    Ga12.3013.3012.3012.813.6015.213.618.820.21816.3018.319.0019.4017.5017.618.80
    Ge2.182.342.062.062.202.072.182.11.571.831.501.771.982.221.912.742.68
    U0.640.660.730.760.760.890.781.271.221.311.181.131.561.651.281.231.29
    Th2.542.742.983.053.203.682.924.785.25.245.024.746.936.065.935.395.70
    下载: 导出CSV

    表  3  样品全岩主量(%)及微量(10-6)元素分析结果

    Table  3.   Major elements and trace elements analysis data

    样品编号5031-1HF-41-15045-1HF-46-2HF-46-45028-25015-15015-35031-35031-35013-4HF-36-7PM07-51-2PM07-51-3PM07-51-4PM07-51-5PM07-51-6
    岩性岩脉岩脉辉长岩辉长闪长岩辉长闪长岩辉长闪长岩辉长闪长岩辉长闪长岩辉长闪长岩辉长闪长岩辉长闪长岩辉长闪长岩闪长岩闪长岩闪长岩闪长岩闪长岩
    SiO239.1145.6241.9048.4442.1747.1947.8247.8142.4442.4444.2449.9250.6950.3850.5951.7951.23
    AI2O310.1810.0610.7613.7513.0714.0314.5014.6215.2215.2215.3013.4215.9616.2115.3415.3915.3
    Fe2O31.631.761.642.602.222.863.362.692.012.012.071.421.781.411.531.731.59
    FeO10.859.829.7510.2510.557.907.907.408.258.258.255.557.848.278.147.947.81
    CaO7.606.207.233.557.195.564.925.647.927.925.077.254.173.964.343.724.4
    MgO10.9711.9612.045.976.645.504.794.434.704.706.906.424.114.194.484.34.21
    K200.310.382.320.480.463.661.922.042.332.333.082.580.340.330.330.310.32
    Na2O0.380.110.693.752.903.534.714.833.843.842.043.895.345.575.455.535.52
    TiO22.922.702.474.154.013.413.072.783.753.753.742.052.742.862.882.962.87
    P2O50.400.410.410.460.430.601.501.520.750.750.760.670.750.830.780.870.8
    MnO0.180.150.160.170.190.160.200.180.170.170.120.120.170.180.170.170.19
    灼失※15.1310.4810.326.139.905.335.085.828.408.408.186.515.965.765.955.255.73
    H2O+3.975.392.183.502.184.442.982.623.203.203.482.162.913.223.232.812.62
    FeOt12.3211.4011.2312.5912.5510.4710.929.8210.0610.0610.116.839.449.549.529.509.24
    Fe2O3t13.712.712.514.013.911.612.110.911.211.211.27.610.510.610.610.610.3
    Mg#65.168.769.249.952.652.447.948.649.549.558.966.447.747.949.748.748.9
    La41.943.453.444.344.773.262.764.967.579.671.177.569.776.374.470.869
    Ce84.288.810691.792.4142134139142166147150154162162152145
    Pr10.21112.311.311.416.316.216.916.519.716.917.418.119.419.418.717.4
    Nd40.243.445.245.246.361.364.266.264.278.263.265.269.673.573.269.266.8
    Sm7.928.478.539.129.4211.813.613.911.916.112.512.212.813.713.813.112.9
    Eu1.922.852.462.452.573.524.124.323.513.793.323.223.913.974.183.743.7
    Gd6.67.167.267.967.89.9512.212.511.214.810.410.410.811.91211.210.9
    Tb0.911.0811.11.121.351.81.791.451.951.461.41.721.711.771.611.59
    Dy4.655.065.085.325.566.838.958.787.310.57.386.948.488.678.918.468.21
    Ho0.820.90.90.961.021.21.631.581.261.791.291.251.541.621.621.561.49
    Er2.062.262.222.382.573.053.963.853.124.153.283.2344.124.063.953.85
    Tm0.280.30.310.330.350.430.540.520.420.530.440.460.580.570.560.550.54
    Yb1.691.81.992.042.042.63.183.212.73.112.692.893.473.543.443.293.32
    Lu0.240.260.280.310.280.380.440.440.40.420.390.440.520.510.490.490.46
    Y19.821.622.322.522.828.139.136.230.742.330.830.634.136.235.634.134
    ∑ REE223.39238.34269.23246.97250.33362.01366.62374.09364.16442.94372.383.13393.32417.71415.43392.75379.16
    LREE186.34197.92227.89204.07206.79308.12294.82305.22305.61363.39314.325.52328.11348.87346.98327.54314.8
    HREE37.0540.4241.3442.943.5453.8971.868.8758.5579.5558.1357.6165.2168.8468.4565 2164.36
    LREE/HREE5.034.905.514.764.755.724.114.435.224.575.405.655.035.075.075.024.89
    Eu*0.791.090.930.860.890.970.960.980.910.740.870.850.990.930.970.920.93
    LaN/YbN17.7817.2919.2515.5815.7220.1914.1414.5017.9318.3618.9619.2414.4115.4615.5115.4414.91
    LaN/SmN3.423.314.043.143.064.002.983.013.663.193.674.103.523.603.483.493.45
    GdN/YbN3.233.293.023.233.163.173.173.223.433.943.202.982.572.782.892.822.72
    Cu89.110611127727214728.226.888.929.491.639.432.432.535.938.732.6
    Pb3.96.041.925.65.210.73.77.016.172.25.0212.15.085.064.325.245.25
    Zn14212611011914916913813012513812584112125114116115
    Cr64972169635.928.327.43.325.31.4317.47.4731.922.313.939.524.420.6
    Ni29434232111411063.15.4915.412.810.418.688.810.38.6318.812.510.5
    Co58.561.153.353.146.134.310.29.9728.2928.728.425.823.825.826.723.9
    Li10839.44834391625.926.525.654.652.819.5122112424440.9
    Rb11.63219129.619.214510396.749.96.380.975.510.59.669.358.68.71
    Cs0.863.9325.31.671.4723.550.232.50.751.241.534.031.411.280.740.730.58
    Sr396240238546667685842957600335238812598614583572613
    Ba15895.7175411405161014401940984155506902397410393398421
    V322283270431457297226197357294347151263264274271258
    Sc2428.825.71819.414.210.412.818.813.9138.3514.313.814.513.815.2
    Nb39.844.148.644.142.671.745.845.765.548.46771.273.77976.87775.5
    Ta2.673.183.243.363.295.013.033.064.53.214.525.125.065.465.295.415.42
    Zr241232252275267421265264326276340433335350374350349
    Hf6.66.326.867.787.510.77.267.358.687.668.7810.69.7610.310.610.510.2
    Be1.071.422.331.41.521.962.181.461.323.11.92.052.62.842.352.822.18
    Ga19.416.817.820.322.4222422.722.826.223.81523.923.724.624.223.6
    Ge2.962.021.861.862.081.621.71.61.392.642.031.421.741.6721.911.72
    U1.21.181.341.171.21.981.41.461.71.391.672.171.822.052.3121.98
    Th4.495.46.385.074.738.516.616.76.777.026.519.117.158.469.848.238.24
    下载: 导出CSV
  • [1] Day J M D, Pearson D G, Hulbert L J. Rhenium-Osmium isotope and platinum-group element constrains on the origin and evolution of the 1.27Ga Muskox layered intrusion[J]. Journal of Petrology, 2008, 49(7):1255~1295. doi: 10.1093/petrology/egn024
    [2] Niu Y L, Wilson M, Humphreys E R, et al. The origin of intra-plate ocean island basalts (OIB):The lid effect and its geodynamic implications[J]. Journal of Petrology, 2011, 52(7/8):1443~1468.
    [3] Spandler C, Mavrogenes J, Arculus R. Orign of chromitiel in layered instrusions:Evidence from hromite-hosted meit inclusion from the still water complex[J]. Geology, 2005, 33:893~896. doi: 10.1130/G21912.1
    [4] Maier W D, Barnes S J, Bandyayera D, et al. Early Kibaran rift-related mafic-ultramafic magmatism in western Tanzania and Burundi:Petrogenesis and ore potential of the Kapalagulu and Musongati layered intrusions[J]. Lithos, 2008, 101(1/2):24~53.
    [5] White R S, Smith L K, Roberts A W. Lower-crustal intrusion on the North Atlantic continental margin[J]. Nature, 2008, 452:460~464. doi: 10.1038/nature06687
    [6] 宋谢炎, 张成江, 胡瑞忠, 等.峨眉火成岩省岩浆矿床成矿作用与地幔柱动力学过程的耦合关系[J].矿物岩石, 2005, 25(4):35~44. http://www.cnki.com.cn/Article/CJFDTOTAL-KWYS200504006.htm

    SONG Xie-yan, ZHANG Cheng-jiang, HU Rui-zhong, et al. Genetic links of magmatic deposits in the Emeishan Large Igneous Province with dynamics of mantle plume[J]. Journal of Mineralogy and Petrology, 2005, 25(4):35~44. http://www.cnki.com.cn/Article/CJFDTOTAL-KWYS200504006.htm
    [7] 徐义刚, 何斌, 罗震宇, 等.我国大火成岩省和地幔柱研究进展与展望[J].矿物岩石地球化学通报, 2013, 32(1):25~39. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH201301003.htm

    XU Yi-gang, HE Bin, LUO Zhen-yu, et al. Study on mantle plume and large igneous provinces in chine:An overview and perspectives[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2013, 32(1):25~39. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH201301003.htm
    [8] Mao J W, Pirajno F, Zhang Z H, et al. A review of the Cu-Ni sulphide deposits in the Chinese Tianshan and Altay orogens (Xinjiang Autonomous Region, NW China):Principal characteristics and ore-forming processes[J]. Journal of Asian Earth Sciences, 2008, 32(2/4):184~203.
    [9] Schilling J G. Upper mantle heterogeneiries and dynamics[J]. Nature, 1985, 314:62~67. doi: 10.1038/314062a0
    [10] Hofmann A W. Mantle geochemistry:The message from oceanic volcanism[J]. Nature, 1997, 385:219~229. doi: 10.1038/385219a0
    [11] 汤耀庆, 肖序常, 赵民.古中亚复合巨型缝合带南缘构造演化[M].北京:科学技术出版社, 1991:109~124.

    TANG Yao-qing, XIAO Xu-chang, ZHAO Min. The tectonic evolution of southern margin of the paleo Asia giant composite suture[M]. Beijing:Science and Technology Press, 1991:109~124.
    [12] 肖序常, 汤耀庆, 李锦轶, 等.新疆北部及邻区大地构造[M].北京:地质出版社, 1992:1~169.

    XIAO Xu-chang, TANG Yao-qing, LI Jin-yi, et al, Tectonics of northern Xinjiang and its adjacent area[M]. Beijing:Geological Publishing House, 1992:1~169.
    [13] 夏林圻, 夏祖春, 徐学义, 等.天山及邻区石炭纪-早二叠世裂谷火山岩岩石成因[J].西北地质, 2008, 04:1~68. doi: 10.3969/j.issn.1009-6248.2008.01.001

    XIA Lin-qi, XIA Zu-chun, XU Xue-yi, et al. Petrogenesis of Caboniferous-Early Permian rift-related volcanic rocks in the Tianshan and its neighboring areas, Northwestern China[J]. Northwestern Geology, 2008, 4:1~68. doi: 10.3969/j.issn.1009-6248.2008.01.001
    [14] 肖序常, 汤耀庆, 王军, 等.中国南天山造山带蓝片岩及其构造意义[J].地球学报, 1994, Z2:54~64. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB4Z2.006.htm

    XIAO Xu-chang, TANG Yao-qing, WANG Jun, et al. Blue schist belts and their tectonic implications of the South Tianshan Mts., NW China[J]. Acta Geologica Sinica, 1994, Z2:54~64. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB4Z2.006.htm
    [15] 蔡东升, 卢华复, 贾东, 等.南天山古生代板块构造演化[J].地质论评, 1995, 05:432~443. doi: 10.3321/j.issn:0371-5736.1995.05.006

    CAI Dong-sheng, LU Hua-fu, JIA Dong, et al. Paleozoic plate tectonic evolution of southern Tianshan[J]. Geological Review, 1995, 05:432~443. doi: 10.3321/j.issn:0371-5736.1995.05.006
    [16] 夏林圻, 张国伟, 夏祖春.天山古生代洋盆开启、闭合时限的岩石学约束-来自震旦纪、石炭纪火山岩的证据[J].地质通报, 2002, 21(2):55~62. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200202001.htm

    XIA Lin-qi, ZHANG Guo-wei, XIA Zi-chun. Constrain on the timing of opening and closing of the Tianshan Paleozoic basin:Evidence from Sinian and Carbonifercous volcanic rocks[J]. Geological Bulletin of China, 2002, 21(2):55~62. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200202001.htm
    [17] Xiao W J, Zhang L C, Qin K Z, et al. Paleozoic accretionary and collisional tectonics of the eastern Tianshan (China):Implications for the continental growth of Central Asia[J]. American Journal of Science, 2004, 304:370~395. doi: 10.2475/ajs.304.4.370
    [18] 李永军, 李注苍, 佟丽莉, 等.论天山古洋盆关闭的地质时限——来自伊宁地块石炭系的新证据[J].岩石学报, 2010, 10:2905~2912. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201010003.htm

    LI Yong-jun, LI Zhu-cang, TONG Li-li, et al. Revisit the constraints on the closure of the Tianshan ancient oceanic basin:New evidence from Yining block of the Carboniferous[J]. Acta Petrologica Sinica, 2010, 10:2905~2912. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201010003.htm
    [19] 李文明, 任秉琛, 杨兴科, 等.东天山中酸性侵入岩浆作用及其地球动力学意义[J].西北地质, 2002, 04:41~64. doi: 10.3969/j.issn.1009-6248.2002.01.005

    LI Wen-ming, REN Bing-chen, YANG Xing-ke, et al. The intermediate-acid intrusive magmatism and its geodynamic significance in Eastern Tianshan region[J]. Northwestern Geology, 2002, 04:41~64. doi: 10.3969/j.issn.1009-6248.2002.01.005
    [20] 江思宏, 聂凤军.北山地区花岗岩类的40Ar/39Ar同位素年代学研究[J].岩石学报, 2006, 11:2719~2732. doi: 10.3969/j.issn.1000-0569.2006.11.010

    JIANG Si-hong, NIE Feng-jun, 40Ar/39Ar geochronology of the granitoids in Beishan Moutain, NW China[J]. Acta Petrologica Sinica, 2006, 11:2719~2732. doi: 10.3969/j.issn.1000-0569.2006.11.010
    [21] 郭瑞清, 秦切, 张晓帆, 等.新疆库鲁克塔格阔克塔格西碱性岩年代学、岩石地球化学特征及其地质意义[J].吉林大学学报:地球科学版, 2013, 02:457~468. http://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ201302014.htm

    GUO Rui-qing, QIN Qie, ZHANG Xiao-fan, et al. Geochronology, petrogeochemistry of western Kuoktagh alkaline rocks in Quruqtagh area in Xinjiang and its geolohical implications[J]. Journal of Jilin University:Earth Science Edition, 2013, 02:457~468. http://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ201302014.htm
    [22] 刘畅, 赵泽辉, 郭召杰.甘肃北山地区煌斑岩的年代学和地球化学及其壳幔作用过程讨论[J].岩石学报, 2006, 05:1294~1306. doi: 10.3321/j.issn:1000-0569.2006.05.019

    LIU Chang, ZHAO Ze-hui, GUO Zhao-jie. Chronology and geochemistry of lamprophyre dykes from Beishan area, Gansu province and implications for the crust-mantle interaction[J]. Acta Petrologica Sinica, 2006, 05:1294~1306. doi: 10.3321/j.issn:1000-0569.2006.05.019
    [23] 张遵忠, 顾连兴, 吴昌志, 等.东天山印支早期尾亚石英正长岩:成岩作用及成岩意义[J].岩石学报, 2006, 05:1135~1149. doi: 10.3321/j.issn:1000-0569.2006.05.007

    ZHANG Zun-zhong, GU Lian-xing, WU Chang-zhi, et al. Weiya quartz syenite in early Indosinina from eastern Tianshan Moutains:Petrogenesis and tectonic implications[J]. Acta Petrologica Sinica, 2006, 05:1135~1149. doi: 10.3321/j.issn:1000-0569.2006.05.007
    [24] 张遵忠, 顾连兴, 吴昌志, 等.中天山东段尾亚印支早-中期石英闪长岩-陆内俯冲与原生下陆壳部分熔融[J].地质学报, 2011, 09:1420~1434. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201109004.htm

    ZHANG Zun-zhong, GU Lian-xing, WU Chang-zhi, et al. Early-Middle Indosinian Weiya quartz diorite, eastern segment of the Middle Tianshan Mountains, NW China:Implications for intra-continent subduction and partial melting of juvenile lower crust[J]. Acta Geologica Sinica, 2011, 09:1420~1434. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201109004.htm
    [25] 朱志新, 董连慧, 王克卓, 等.西天山造山带构造单元划分与构造演化[J].地质通报, 2013, Z1:297~306. doi: 10.3969/j.issn.1671-2552.2013.02.009

    ZHU Zhi-xin, DONG Lian-hui, WANG Ke-zhuo, et al. Tectonic division and regional tectonic evolution of West Tianshan organic belt[J]. Geological Bulletin of China, 2013, Z1:297~306. doi: 10.3969/j.issn.1671-2552.2013.02.009
    [26] 邹亚锐, 塔吉古丽, 邢作云, 等.塔里木新元古代-古生代沉积盆地演化[J].地球科学:中国地质大学学报, 2014, 08:1200~1216. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201408020.htm

    ZOU Ya-rui, TAJI Gu-li, XING Zuo-yun, et al. Evolution of sedimentary basins in Tarim during Neoprpterpzoic-Paleozoic[J]. Earth Science:Journal of China University of Geosciences, 2014, 08:1200~1216. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201408020.htm
    [27] 高小芬, 林晓, 徐亚东, 等.南天山古生代-中生代沉积盆地演化[J].地球科学:中国地质大学学报, 2014, 08:1119~1128. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201408013.htm

    GAO Xiao-fen, LIN Xiao, XU Ya-dong, et al. Evolution of sedimentary basins in South Tianshan during Paleozoic-Mesozoic[J]. Earth Science:Journal of China University of Geosciences, 2014, 08:1119~1128. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201408013.htm
    [28] 杨树锋, 陈汉林, 厉子龙, 等.塔里木早二叠世大火成岩省[J].中国科学:地球科学, 2014, 02:187~199. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201402001.htm

    YANG Shu-feng, CHEN Han-lin, LI Zi-long, et al. Early Permian Tarim Large Igneous Province in northwest China[J]. Science in China:Earth Sciences, 2014, 02:187~199. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201402001.htm
    [29] Andersen T. Correction of common lead in U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 2002, 192:59~79. doi: 10.1016/S0009-2541(02)00195-X
    [30] Luddwig KR. Isoplot:A plotting and regression program for radiogenic-isotope data[R]. US Geological Survey Open-File Report, 1991:91~445.
    [31] Rubatto D. Zircon trace element geochemistry:Partitioning with garnet and the link between U-Pb ages and metamorphism[J]. Chemical Geology, 2002, 184:123~138. doi: 10.1016/S0009-2541(01)00355-2
    [32] Winchester J A, Floyd P A. Geochemical discrimination of different magma series and their differentiation products using immobile elements[J]. Chemical Geology, 1977, 20:325~343. doi: 10.1016/0009-2541(77)90057-2
    [33] Sun S, Mcdonough W F. Chemical and isotopic systematics of oceanic Sun S, Mcdonough W F. Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes[J]. Geological Society, London, Special Publications, 1989, 42(1):313~345. doi: 10.1144/GSL.SP.1989.042.01.19
    [34] 邓宇峰, 宋谢炎, 陈列锰, 等.东天山黄山西含铜镍矿镁铁-超镁铁岩体岩浆地幔源区特征研究[J].岩石学报, 2011, 27(12):3640~3652. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201112012.htm

    DENG Yu-feng, SONG Xie-yan, CHEN Lie-meng, et al. Features of the mantle source of the Huangshanxi Ni-Cu sulfide-bearing mafic-ultramafic intrusion, eastern Tianshan[J]. Acta Petrologica Sinica, 2011, 27(12):3640~3652. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201112012.htm
    [35] Ao S J, Xiao W J, Han C M. Geochronology and geochemistry of early Permian mafic-ultramafic complexes in the Beishan area, Xinjiang, NW China:Implications for late Paleozoic tectonic evolution of the southern Altaids[J]. Gondwana Research, 2010, 1:004.
    [36] 姜常义, 贾承造, 李良辰.新疆麻扎尔塔格地区铁富集型高镁岩浆的源区[J].地质学报, 2004, 78(6):770~780. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200406007.htm

    JIANG Chang-yi, JIA Cheng-zao, LI Liang-chen. Source of the Fe-riched-type high-Mg magma in Mazhartag Region, Xinjiang[J]. Acta Geologica Sinica, 2004, 78(6):770~780. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200406007.htm
    [37] 张传林, 周刚, 王洪燕, 等.塔里木和中亚造山带西段二叠纪大火成岩省的两类地幔源区[J].地质通报, 2010, 29(6):779~794. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201006002.htm

    ZHANG Chuan-lin, ZHOU Gang, WANG Hong-yan, et al. A review on two types of mantle domains of the Permian large igneous province in Tarim and the western section of Central Asian orogenic belt[J]. Geological Bulletin of China, 2010, 29(6):779~794. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201006002.htm
    [38] 喻学惠, 赵志丹, 莫宣学, 等.甘肃西秦岭新生代钾霞橄黄长岩和碳酸岩的微量、稀土和Sr, Nd, Pb同位素地球化学:地幔柱-岩石圈交换的证据[J].岩石报报, 2004, 3:483~494. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200403012.htm

    YU Xue-hui, ZHAO Zhi-dan, MO Xuan-xue, et al. Trace elements, REE and Sr, Nd, Pb isotopic geochemistry of Cenozoic kamafugite and carbonatite from west Qinling, Gamsu province:Implication of plume-liyhosphere interaction[J]. Acta Petrologica Sinica, 2004, 3:483~494. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200403012.htm
    [39] Woodhead J D, Hergt J M, Davidson J P. Hafnium isotope evidence for conservative element mobility during subduction zone processes. Earth and Planetary Science Letters, 2001, 192(3):331~346. doi: 10.1016/S0012-821X(01)00453-8
    [40] Le Roex A O, Dick H J B. Geochemistry, mineralogy and petrogenensis of levaserupted along the southwest Indian Ridge between the Bouvet tripe junction and 11 degrees east[J]. Journal of Petrology, 2003, 24(3):267~318.
    [41] Wang K, Plant T, Walker J D. A mantle melting profile across the basin and range, SW USA[J]. Journal of Geophysical Research, 2002, 107(10):1029.
    [42] Hardarson B S, Fitton J G. Increased mantle melting beneath Snaefellsjokull volcano during Late Pleistocene deglaciation[J]. Nature, 1991, 353:62~64. doi: 10.1038/353062a0
    [43] 钟宏, 胡瑞忠, 朱维光.层状岩体的成因及成矿作用[J].地学前缘, 2007, 14(2):159~172. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200702012.htm

    ZHONG Hong, HU Rui-zhong, ZHU Wei-guang. Genesis and mineralization of layered intrusions[J]. Earth Science Frontiers, 2007, 14(2):159~172. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200702012.htm
    [44] Green D H. Genesis of archean peridotitic magmas and constraints on archean geothermal gradients and tectonics[J]. Geology, 1975, 3:15~18. doi: 10.1130/0091-7613(1975)3<15:GOAPMA>2.0.CO;2
    [45] Hess P C. Phase equilibria constraints on the origin of ocean floor basalts[C]//Morgan J P, Blackman D K, Sinton J M. Mantle flow and melt generation at mid-ocean ridges.Geophysical Monograph, American Geophysical Union, 1992, 71:67~102.
    [46] Frey F A, Green D H, Roy S D. Integrated models of basalts petrogenesis:A study of quartz tholeiites to olivine melilitites from south eastern Australia utilizing geochemical and experimental petrological data[J]. Journal of Petrolog y, 1978, 19:463~513. doi: 10.1093/petrology/19.3.463
    [47] Macdonald R, Rogers N W, Fitton J G. Plume-lithosphere interactions in the generation of the basalts of the Kenya Rift, East Africa[J]. Journal of Petrology, 2001, 42:877~900. doi: 10.1093/petrology/42.5.877
    [48] Hofmann W. Chemical differentiation of the earth:The realationship between mantle, continental crust and oceanic crust[J]. Earth and Planetary Science Letters, 1986, 90:297~314.
    [49] Sun S S, Mcdonough W F. Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes[J]. Geological Society, London, Special Publications, 1989, 42(1):313~345. doi: 10.1144/GSL.SP.1989.042.01.19
    [50] 韩吟文, 马振东, 张宏飞.地球化学[M].第二版.北京:地质出版社, 2003:227~228.

    HAN Yin-wen, MA Zhen-dong, ZHANG Hong-fei. Geochemistry[M]. Beijing:Geological Publishing House, 2003:227~228.
    [51] Toplis M J, Carroll M R. An experimental study of the influence of oxygen fugacity on Fe-Ti oxide stability, phase relations, and mineral-melt equilibria in ferrobasaltic systems[J].Journal of Petrology, 1995, 36:1137~1170. doi: 10.1093/petrology/36.5.1137
    [52] 杨树锋, 余星, 陈汉林, 等.塔里木盆地巴楚小海子二叠纪超基性脉岩的地球化学特征及其成因探讨[J].岩石学报, 2007, 23(5):1087~1096. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200705022.htm

    YANG Shu-feng, YU Xing, CHEN Han-lin, et al. Geochemical characteristics and petrogenesis of Permian Xiaohaizi ultrabasic dyke in Bachu area, Tarim basin[J]. Acta Petrologica Sinica, 2007, 23(5):1087~1096. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200705022.htm
    [53] 励音骐, 厉子龙, 孙亚莉励音骐, 厉子龙, 孙亚莉, 等.塔里木瓦吉里塔格超镁铁质隐爆角砾岩铂族元素和微量元素地球化学特征及其岩石成因探讨[J].岩石学报, 2010, 11:3307~3318. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201011013.htm

    LI Yin-qi, LI Zi-long, SUN Ya-li, et al. PGE and geochemistry of Wajilitag ultramafic cryptoexplosive brecciated rocks from Tarim Basin:Implicatons for petrogenesis[J].Acta Petrologica Sinica, 2010, 11:3307~3318. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201011013.htm
    [54] 陈汉林, 杨树锋, 厉子龙, 等.塔里木盆地二叠纪大火成岩省发育的时空特点[J].新疆石油地质, 2009, 30(2):179~182. http://www.cnki.com.cn/Article/CJFDTOTAL-XJSD200902013.htm

    CHEN Han-lin, YANG Shu-feng, LI Zi-long, et al. Spatial and temporal characteristics of Permian Large Igneous Province in Tarim Basin[J]. Xinjiang Petroleum Geology, 2009, 30(2):179~182. http://www.cnki.com.cn/Article/CJFDTOTAL-XJSD200902013.htm
    [55] Wei X, Xu Y G, Luo Z Y, et al. Composition of the Tarim mantle plume:Constraints from clinopyroxene antecrysts in the early Permian Xiaohaizi dykes, NW China[J]. Lithos, 2015, 205:69~81.
    [56] Xu Y G, Wei X, Luo Z Y, et al. The Early Permian Tarim Large Igneous Province:Main characteristics and a plume incubation model[J]. Lithos, 2014, 204:20~35. doi: 10.1016/j.lithos.2014.02.015
    [57] Agust Gudmundsson, Ingrid F Loetveit. Dyke emplacement in a layered and faulted rift zone[J]. Journal of Volcanology and Geothermal Research, 2005, 144(1/4):311~327.
    [58] Kiselev A I, Ernst R E, Yarmolyuk V V, et al. Radiating rifts and dyke swarms of the middle Paleozoic Yakutsk plume of eastern Siberian Craton[J]. Journal of Asian Earth Sciences, 2012, 45:1~16. doi: 10.1016/j.jseaes.2011.09.004
    [59] 曾广策, 邱家骧.碱性岩的概念及其分类命名综述[J].地质科技情报, 1996, 01:31~37. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ199601009.htm

    ZENG Guang-ce, QIU Jia-xiang, Conception of alkaline rocks and their nomenclature[J]. Geological Science and Technology Information, 1996, 01:31~37. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ199601009.htm
    [60] 李曰俊, 孙龙德, 吴浩若, 等.中国南天山西端乌帕塔尔坎群发现石炭纪一二叠纪放射虫化石[J].地质科学, 2005, 40(2):220~226. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200501017.htm

    LI Yue-jun, SUN Long-de, WU Hao-ruo, et al. Permo-Carboniferous radiolaria from the Wupatarkan Group, west terminal of Chinese south Tianshan[J]. Chinese Journal of Geology, 2005, 40(2):220~226. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200501017.htm
    [61] 李曰俊, 杨海军, 赵岩, 等.南天山区域大地构造与演化[J].大地构造与成矿学, 2009, 33(1):94~104. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200901013.htm

    LI Yue-jun, YANG Hai-jun, ZHAO Yan, et al. Tectonic framework and evolution of south Tianshan, NW China[J]. Geotectonica et Metallogenia, 2009, 33(1):94~104. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200901013.htm
    [62] 张立飞, 杜瑾雪, 吕增, 等.新疆西南天山超高压变质带的空间分布、峰期变质时代和P-T轨迹特征[J].科学通报, 2013, 22:2107~2112. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201322000.htm

    ZHANG Li-fei, DU Jin-xue, LÜ Zeng, et al. A huge oceanic-type UHP metamorphic belt in southwestern Tianshan, China:Peak metamorphic age and P-T path[J].Chinese Science Bulletin, 2013, 22:2107~2112. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201322000.htm
    [63] 郑建平, 罗照华, 余淳梅, 等.新疆托云麻粒岩捕虏体地球化学和锆石年代学:岩石成因及西南天山下地壳性质[J].科学通报, 2005, 50(12), 1242~1251. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200508012.htm

    ZHENG Jian-ping, LUO Zhao-hua, YU Chun-mei, et al. Geochemistry and zircon U-Pb ages of granulite xenolith from Tuoyun basalts, Xinjiang:Implications for the petrogenesis and the lower crustal nature beneath the southwestern Tianshan[J].Chinese Science Bulletin, 2005, 50(12), 1242~1251. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200508012.htm
    [64] Henderson P. Rare earth element geochemistry[M]. Netherlands:Elsevier Science Publishers B V, 1984:23~28.
    [65] 罗金海, 车自成, 周新源, 等.塔里木盆地西部中生代早期伸展作用的辉绿岩证据[J].中国地质, 2006, 33(3):566~571. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200603012.htm

    LUO Jin-hai, CHE Zi-cheng, ZHOU Xin-yuan, et al. Diabase evidence for the early Mesozoic extension in the western Tarim basin, NW China[J]. Geology In China, 2006, 33(3):566~571. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200603012.htm
  • 加载中
图(10) / 表(3)
计量
  • 文章访问数:  195
  • HTML全文浏览量:  95
  • PDF下载量:  6
  • 被引次数: 0
出版历程
  • 收稿日期:  2016-09-12
  • 刊出日期:  2016-12-01

目录

    /

    返回文章
    返回